Rock Identifier
Labradorite (Labradorite, a plagioclase feldspar in the albite–anorthite series, approximately (Ca,Na)(Al,Si)₄O₈) — mineral
mineral

Labradorite

Labradorite, a plagioclase feldspar in the albite–anorthite series, approximately (Ca,Na)(Al,Si)₄O₈

AI-generated identification · may be incorrect

Dark gray, polished specimen showing blue-green and orange labradorescence; vitreous luster, triclinic crystals, two cleavage directions, Mohs hardness 6–6.5, and specific gravity about 2.7. The iridescent flash is visible as light reflects from internal layers.

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Physical properties

Dark gray, polished specimen showing blue-green and orange labradorescence; vitreous luster, triclinic crystals, two cleavage directions, Mohs hardness 6–6.5, and specific gravity about 2.7. The iridescent flash is visible as light reflects from internal layers.

Formation & geological history

Forms as calcium-rich plagioclase in cooling mafic igneous rocks, especially gabbro and anorthosite; these rocks are Precambrian in many well-known deposits. The image alone does not establish the specimen’s locality or age.

Uses & applications

Polished labradorite is used for jewelry, beads, carvings, and decorative objects; plagioclase is also a major rock-forming mineral.

Geological facts

Its shifting color effect is called labradorescence, produced by light interference within fine internal compositional layers.

Field identification & locations

Rotate the stone under a point light to reveal broad, shifting flashes; this polished piece is consistent with labradorite, though identification from an image is not definitive. Notable sources include Labrador, Canada, Madagascar, Finland, and Norway.